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Par Collection Par Auteur- KUHLE, M. (3)
- Allemagne RFA ; Biotope ; Carte au 1 : 25 000 ; Carte géomorphologique ; Cartographie ; Concept ; Ecologie ; Géographie physique ; Méthodologie ; Réduction (1)
- Asia ; Erratic boulder ; Glacial isostasy ; Glaciation ; Ground moraine ; Model ; Mountain ; Palaeoclimatology ; Quaternary ; Tibet ; Vertical movement (1)
- Asia ; Geochronology ; Glaciation ; Glacier ; Grain size distribution ; Himalaya ; Lateglacial ; Mass movement ; Model ; Moraine ; Palaeogeography ; Roche moutonnée ; Snow ; Snow line ; Tibet ; Vertical movement (1)
- Asie ; Bloc erratique ; Glaciation ; Glacio-isostasie ; Modèle ; Montagne ; Moraine de fond ; Mouvement vertical ; Paléoclimatologie ; Quaternaire ; Tibet (1)
- Asie ; Glaciation ; Glacier ; Granulométrie ; Géochronologie ; Himalaya ; Limite d'enneigement ; Modèle ; Moraine ; Mouvement de masse ; Mouvement vertical ; Neige ; Paléogéographie ; Roche moutonnée ; Tardiglaciaire ; Tibet (1)
- Physical geography (1)
- Glacial isostatic uplift of Tibet as a consequence of a former ice sheet (1)
- New findings concerning the Ice Age (Last Glacial Maximum) glacier cover of the East-Pamir, of the Nanga Parbat up to the Central Himalaya and of Tibet, as well as the age of the tibetan inland ice (1)
- Quantificational reductionism as a risk in geography and cartography instanced by the 1 : 25 000 geomorphological map of the Federal Republic of Germany (1)
- Tibet and High-Asia (1)
- A reductionistic concept is being pursued in the 1/25 000 geomorphological mapping of the Federal Republic of Germany. This reduction has proved to be too drastic insofar as it gives rise to irretrievable loss of information. The claim that use
- the course of the Pleistocene the High Plateau was glaciated several times so that at each time here alternated a maximum glacial isostatic depression and an interglacial uplift, such as that resulting again today. This is proved by the ground and end
- is proved; a snow-line (ELA)-depression of 820-1250 m in relation to the present relief has been calculated. Modelling by means of those snow-line depressions and estimations of the precipitation provide ideas about surface heights, ice thicknesses and flow